Pensacola Mountains
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The Pensacola Mountains () are a large group of mountain ranges and peaks that extend in a northeast–southwest direction in the
Transantarctic Mountains The Transantarctic Mountains (abbreviated TAM) comprise a mountain range of uplifted rock (primarily sedimentary) in Antarctica which extends, with some interruptions, across the continent from Cape Adare in northern Victoria Land to Coats L ...
System, Queen Elizabeth Land region of Antarctica. They comprise the Argentina Range, Forrestal Range, Dufek Massif, Cordiner Peaks, Neptune Range, Patuxent Range, Rambo Nunataks and Pecora Escarpment. These mountain units lie astride the extensive Foundation Ice Stream and Support Force Glacier which drain northward to the Ronne Ice Shelf.


Discovery and naming

The Pensacola Mountains were discovered and photographed on 13 January 1956 in the course of a transcontinental nonstop plane flight by personnel of
United States Navy The United States Navy (USN) is the naval warfare, maritime military branch, service branch of the United States Department of Defense. It is the world's most powerful navy with the largest Displacement (ship), displacement, at 4.5 millio ...
Operation Deep Freeze Operation Deep Freeze is the code name for a series of United States missions to Antarctica, beginning with "Operation Deep Freeze I" in 1955–56, followed by "Operation Deep Freeze II", "Operation Deep Freeze III", and so on. (There was an init ...
I from McMurdo Sound to
Weddell Sea The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and the Antarctic Peninsula. The easternmost point is Cape Norvegia at Princess Martha C ...
and return. They were named by the United States
Advisory Committee on Antarctic Names The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established ...
(US-ACAN) for the U.S. Naval Air Station,
Pensacola, Florida Pensacola ( ) is a city in the Florida panhandle in the United States. It is the county seat and only incorporated city, city in Escambia County, Florida, Escambia County. The population was 54,312 at the 2020 United States census, 2020 census. ...
, in commemoration of the historic role of that establishment in training aviators of the United States Navy. The mountains were mapped in detail by
United States Geological Survey The United States Geological Survey (USGS), founded as the Geological Survey, is an agency of the U.S. Department of the Interior whose work spans the disciplines of biology, geography, geology, and hydrology. The agency was founded on Mar ...
(USGS) from surveys and United States Navy air photos in 1956–67.


Geology

The Pensacola Mountains were originally continuous with the Ventana Mountains near
Bahía Blanca Bahía Blanca (; English: ''White Bay''), colloquially referred to by its own local inhabitants as simply Bahía, is a city in the Buenos Aires Province, Buenos Aires province of Argentina, centered on the northwestern end of the eponymous Blanc ...
in
Argentina Argentina, officially the Argentine Republic, is a country in the southern half of South America. It covers an area of , making it the List of South American countries by area, second-largest country in South America after Brazil, the fourt ...
, Cape Fold Belt in
South Africa South Africa, officially the Republic of South Africa (RSA), is the Southern Africa, southernmost country in Africa. Its Provinces of South Africa, nine provinces are bounded to the south by of coastline that stretches along the Atlantic O ...
, the Ellsworth Mountains (West Antarctica) and the Hunter-Bowen orogeny in eastern
Australia Australia, officially the Commonwealth of Australia, is a country comprising mainland Australia, the mainland of the Australia (continent), Australian continent, the island of Tasmania and list of islands of Australia, numerous smaller isl ...
. The
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years f ...
-
Devonian The Devonian ( ) is a period (geology), geologic period and system (stratigraphy), system of the Paleozoic era (geology), era during the Phanerozoic eon (geology), eon, spanning 60.3 million years from the end of the preceding Silurian per ...
Neptune Group rests unconformably on a Cambrian succession, and is overlain disconformably by the Dover
Sandstone Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ...
of the Beacon Supergroup. Within the Neptune Group is the Brown Ridge Conglomerate, Elliott Sandstone, Elbow Formation, and the Heiser Sandstone.


Western features

The Foundation Ice Stream flows through the western part of the range. File:Pecora Escarpment USGS.jpg, Pecora Escarpment, South tip of Patuxent Range File:Thomas Hills USGS.jpg, Patuxent Range. Rambo Nunataks to north File:C83052s5 Schmidt Hills.jpg, North part of Neptune range * Pecora Escarpment (), an irregular escarpment, long, standing southwest of Patuxent Range and marking the southernmost exposed rocks of the Pensacola Mountains. * Patuxent Range (), a major range of the Pensacola Mountains. It comprises the Thomas Hills, Anderson Hills, Mackin Table and various
nunatak A nunatak (from Inuit language, Inuit ) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also cal ...
s and ridges bounded by the Foundation Ice Stream, Academy Glacier and the Patuxent Ice Stream. * Rambo Nunataks (), a loose chain of
nunatak A nunatak (from Inuit language, Inuit ) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also cal ...
s which lie northwest of Patuxent Range and extend along the west side of the Foundation Ice Stream for . * Neptune Range (), a mountain range, long, lying west-southwest of Forrestal Range in the central part of the Pensacola Mountains. The range comprises Washington Escarpment with its associated ridges, valleys and peaks, the Iroquois Plateau, the Schmidt Hills and Williams Hills.


Northern features

The northern part of the range is to the south of the Filchner–Ronne Ice Shelf. File:C82052s5 Ant.Map Cordiner Peaks.jpg, Cordiner Peaks, West part of Dufek Massif File:C82045s1 Ant.Map Davis Valley cropped.jpg, East part of Dufek Massif. North part of Forrestal Range File:Saratoga Table USGS.jpg, South part of Forrestal Range File:C82037s5 Ant.Map Argentina Range.jpg, Argentina Range * Cordiner Peaks (), a group of peaks extending over an area of standing southwest of Dufek Massif in the northern part of the Pensacola Mountains. * Dufek Massif (), a rugged, largely snow-covered
massif A massif () is a principal mountain mass, such as a compact portion of a mountain range, containing one or more summits (e.g. France's Massif Central). In mountaineering literature, ''massif'' is frequently used to denote the main mass of an ...
long, standing west of the Forrestal Range in the northern part of the Pensacola Mountains. * Forrestal Range (), a largely snow-covered
mountain range A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have aris ...
, about long, standing east of Dufek Massif and the Neptune Range in the Pensacola Mountains. * Argentina Range (), a range of rock peaks and bluffs, long, lying east of the northern part of Forrestal Range in the northeastern portion of the Pensacola Mountains.


References


Sources

* * *


Further reading

* Gunter Faure, Teresa M. Mensing,
The Transantarctic Mountains: Rocks, Ice, Meteorites and Water
', P 233 * M.J.Bentley, A.S.Hein, D.E.Sugden, P.L.Whitehouse, R.Shanks, S.Xu, S.P.H.T.Freeman,
Deglacial history of the Pensacola Mountains, Antarctica from glacial geomorphology and cosmogenic nuclide surface exposure dating
', Quaternary Science Reviews Volume 158, 15 February 2017, Pages 58–76, https://doi.org/10.1016/j.quascirev.2016.09.028 * JOHN C. BEHRENDT, JOHN R. HENDERSON, LAURENT ElSTER, and WILLIAM L. RAMBO,
Geophysical Investigations of the Pensacola Mountains and Adjacent Glacierized Areas of Antarctica
', GEOLOGICAL SURVEY PROFESSIONAL PAPER 844 * Curtis, M. (2002),
Palaeozoic to Mesozoic polyphase deformation of the Patuxent Range, Pensacola Mountains, Antarctica
', Antarctic Science, 14(2), 175–183. https://doi:10.1017/S0954102002000743 * Myrl E. Beck, ''Palaeomagnetism and Magnetic Polarity Zones in the Jurassic Dufek Intrusion, Pensacola Mountains, Antarctica'', Geophysical Journal International, Volume 28, Issue 1, May 1972, Pages 49–63, https://doi.org/10.1111/j.1365-246X.1972.tb06110.x * Hodgson, Dominic A Bentley, Michael J,
Lake highstands in the Pensacola Mountains and Shackleton Range 4300–2250 cal. yr BP: Evidence of a warm climate anomaly in the interior of Antarctica
', https://doi.org/10.1177/0959683612460790 * Karolien Peeters (UGent), Dominic A Hodgson, Peter Convey and Anne Willems (UGent),
Culturable diversity of heterotrophic bacteria in Forlidas Pond (Pensacola Mountains) and Lundström Lake (Shackleton Range), Antarctica
', (2011) MICROBIAL ECOLOGY. 62(2). p. 399-413 {{refend Mountain ranges of Queen Elizabeth Land Transantarctic Mountains